Rossby Award 2006 Winner Thesis Abstract
The Diurnal
Cycle of Air Pollution in the Kathmandu Valley, Nepal
by Arnico Panday
Abstract:
This dissertation describes the most
comprehensive study to date of the diurnal cycle of air
pollution in the Kathmandu Valley, Nepal--a bowl-shaped
mountain valley of two million people with a growing air
pollution problem but little past research. Field
measurements and computer simulations were used to study the
interplay of emissions and ventilation.
From
September, 2004, through June 2005, CO (Carbon monoxide), ozone,
PM10 (particles
smaller than 10 micrometers), wind speed and direction, solar
radiation, temperature and humidity were continuously measured
east of Kathmandu. Sensors towers and mountains measured
the diurnal cycle of the vertical temperature structure and
stability. A sodar measured the mixed layer height and
upper-level winds. Bag sampling provided the diurnal cycle
of CO on mountains, passes and around the valley. Winds
were measured on a mountain pass and ozone on a mountaintop.
Patterns of air pollution and meteorology in the valley showed
remarkable day-to-day similarity, with daily twin peaks of CO
and PM10, a noon
ozone maximum, afternoon westerly winds, and a stagnant cold
pool at night. On mountaintops at night, ozone remained
high, while CO dropped to regional background levels.
The meso-scale
meteorological model MM5 was adapted to the Kathmandu Valley for
days in February and May, 2005. It was able to capture the
essential features of the valley's meteorology and was used to
address three specific questions: The break-up of the
valley's temperature inversion was found to be dominated in
February by up-slope winds on the valley rim, plus subsidence
over the valley center; in May, surface heating of the
valley bottom also played a major role. The pathways of
pollutant transport out of the valley were found to be up the
valley rim slopes in the morning, but out the eastern and
southern passes in the afternoons. At night, pollutants
remained within the valley except near the river outlet.
They were lifted off the ground at night and re-circulated in
the morning.
The eulerian chemistry transport model CAMx,
was used in tracer mode, with MM5 meteorology to simulate the
emission, transport and removal of CO from the Kathmandu
inventory, especially the spatial distribution of emissions.